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A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS

Wilson, J. Tuzo·1963·Canadian Journal of Physics

Abstract

It is noted that different physicists and geologists have in recent years espoused not less than four groups of theories of the physical behavior of the Earth's interior. Recent observations of submarine geology, heat, and rock magnetism have tended to support some form of continental drift rather than the older concept of a rigid earth.The Hawaiian Islands are one of seven, parallel, linear chains of islands and seamounts in the Pacific Ocean of Tertiary to Recent age. Their nature had previously been explained in terms of a series of volcanoes along parallel faults. Horizontal shear motion along these faults was supposed to be extending them southeasterly.The inadequacies of this explanation are pointed out. If there are convection currents in the Pacific region and if the upper parts of these cells move faster than the central parts, sources of lava within the slower moving cores could give rise to linear chains of progressively older volcanic piles such as the Hawaiian Islands. This view is shown to be compatible with seismic observations and age determinations.

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Research works printed but not linked: 27

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Metadata

Authors
Wilson, J. T.
Venue
Canadian Journal of Physics
Published
1963-06-01
Volume
41
Issue
6
Pages
863-870
ISSN
  • 0008-4204 (ISSN-L)
  • 1208-6045
OpenAlex
W2099199436
Cited by
1,185
References
0
FWCI
6.37
Type
journal article
Language
en
Open access
closed
Licence
www.nrcresearchpress.com/page/about/CorporateTextAndDataMining (tdm)

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CoChat. (2026). Citation check: A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS. https://app.cochat.ai/papers/10.1139/p63-094
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Wilson, J. T. (1963). A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS. Canadian Journal of Physics. https://doi.org/10.1139/p63-094

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